2021
DOI: 10.1016/j.ecss.2021.107476
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Land-based sediment sources and transport to southwest Puerto Rico coral reefs after Hurricane Maria, May 2017 to June 2018

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Cited by 13 publications
(12 citation statements)
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“…The degree to which terrestrial sediments discharged from watersheds can potentially influence coral reefs depends not only on watershed processes controlling erosion, deposition and discharge but also on the level of connectivity between watersheds and coral reefs (Bainbridge et al, 2018). Throughout the USVI and PR, studies have shown that watersheds can exert an influence on coral environments through the following approaches: (a) spatial distribution of coral species ranked by perceived level of sediment tolerance in relation to distance from watershed outlets (e.g., Acevedo et al, 1989); (b) a proven temporal synchrony between measured seasonal watershed runoff and isotopic signals of dissolved inorganic carbon in coral cores (Moyer and Grottoli, 2011); (c) decreases in net skeletal growth rates determined from coral cores associated with seasonal increases in watershed runoff (Miller and Cruise, 1995); (d) mineralogical fingerprinting of sediment sources (Takesue et al, 2021); and (e) sediment plume mapping using remotely sensed techniques (Hernández et al, 2020). However, none of these studies have demonstrated temporal trends in coral reef conditions in response to changes in sediment discharge corresponding to varying land use, extreme events, or the implementation of erosion mitigation strategies.…”
Section: General Backgroundmentioning
confidence: 99%
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“…The degree to which terrestrial sediments discharged from watersheds can potentially influence coral reefs depends not only on watershed processes controlling erosion, deposition and discharge but also on the level of connectivity between watersheds and coral reefs (Bainbridge et al, 2018). Throughout the USVI and PR, studies have shown that watersheds can exert an influence on coral environments through the following approaches: (a) spatial distribution of coral species ranked by perceived level of sediment tolerance in relation to distance from watershed outlets (e.g., Acevedo et al, 1989); (b) a proven temporal synchrony between measured seasonal watershed runoff and isotopic signals of dissolved inorganic carbon in coral cores (Moyer and Grottoli, 2011); (c) decreases in net skeletal growth rates determined from coral cores associated with seasonal increases in watershed runoff (Miller and Cruise, 1995); (d) mineralogical fingerprinting of sediment sources (Takesue et al, 2021); and (e) sediment plume mapping using remotely sensed techniques (Hernández et al, 2020). However, none of these studies have demonstrated temporal trends in coral reef conditions in response to changes in sediment discharge corresponding to varying land use, extreme events, or the implementation of erosion mitigation strategies.…”
Section: General Backgroundmentioning
confidence: 99%
“…Estimates of the amount of sediment mobilized by landslides during Hurricane María indicate that landsliding is more important than surface erosion within RLGB (Ramos-Scharrón et al, 2021). In addition, recent geochemical evidence has proven a connection between sediments being delivered by watersheds draining to the coastline ∼15 km east from coral reefs off Guánica Bay (Takesue et al, 2021). This sediment connectivity had been recognized only anecdotally in the past (Acevedo et al, 1989).…”
Section: Río Loco-guánica Bay Puerto Ricomentioning
confidence: 99%
“…Particularly, the coastal environment of Florida is advantageous to tidal flat accretion, which makes this state an ideal place to implement the case study. First, Florida is the most hurricane-prone state in the US [36,37], and numerous studies [38][39][40][41][42][43][44] agree that hurricanes could bring in tremendous sediments along the coast. Second, over a half of the coastal wetlands in the conterminous US are distributed along the Gulf Coast [45].…”
Section: Study Areamentioning
confidence: 99%
“…The coral reefs condition in the Caribbean has declined because of the acute and direct effects of human activities, including eutrophication and dredging. These disturbances have produced a high decrease in coral cover, accompanied by changes in the relative abundance of coral species, reduced species diversity, and a shift to slower-growing coral species which is directly related to the tolerance of individual species to sediment stress ( Larsen & Webb, 2009 ; Ramos-Scharrón, Torres-Pulliza & Hernández-Delgado, 2015 ; Takesue et al, 2021 ). The negative effects on corals are exacerbated by stresses from global changes, such as bleaching in response to rising sea temperatures ( Hughes et al, 2018a ; Hughes et al, 2018b ), reduced calcification in organisms due to ocean acidification ( Albright et al, 2016 ; Courtney et al, 2020 ), and more frequent storm damage ( Manfrino et al, 2013 ).…”
Section: Introductionmentioning
confidence: 99%